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A Taxonomic Survey of Seaweeds from Eritrea

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A Taxonomic Survey of Seaweeds from Eritrea BLUMEA 50: 65–111 Published on 22 April 2005 http://dx.doi.org/10.3767/000651905X623292 A TAXONOMIC SURVEY OF SEAWEEDS FROM ERITREA M. ATEWEBERHAN1 & W.F. PRUd’hoMME VAN REINE2 SUMMARY A survey of seaweeds was made in Eritrea in December 1995 and January 1996 on some islands of the Dahlak Archipelago and the surroundings of the port town of Massawa. During our study 101 specific and infraspecific taxa were identified, including 26 Chlorophyta, 20 Phaeophyta and 55 Rhodophyta. The survey resulted in 36 new records for Eritrea (11 Chlorophyta, 7 Phaeophyta and 18 Rhodophyta). Of these Eritrean records, 26 are new for the Red Sea (5 Chlorophyta, 4 Phaeophyta and 17 Rhodophyta). Comparison of records of seaweeds from localities in Eritrea to those from other localities in Eritrea as well as from other coasts of the western Indian Ocean have revealed that the regional distribution of seaweeds in the Red Sea is very patchy and that generally the area seems to be undersampled. The comparisons have also underscored the stressful seasonal environmental conditions for macroalgae in the southern Red Sea. Key words: benthic marine macroalgae, biogeography, Eritrea, Red Sea, taxonomy. ERITREA AND ITS SEAWEEDS INTRODUCTION The environment The coastal zone of Eritrea lies in the southern part of the Red Sea and it is just over 1000 km long, excluding the Dahlak Archipelago. In older literature the coast of Eritrea is often named as the Ethiopian Red Sea coast. The maritime environment is control- led by the Indian Ocean monsoon system resulting in two distinct seasons: the cold season (north-eastern monsoon, October to April) and the hot season (south-western monsoon, May to September). Locally, winds blow to the north-west during the cold season and to the south-east in the hot season. Surface currents are in accordance with prevailing winds (Morcos, 1970). Lower water temperatures, greater water movement, higher nutrient levels and greater planktonic primary productivity are characteristic of the north-eastern monsoon. The parameters are reversed during the south-western monsoon (Morcos, 1970; Lipkin, 1987, 1991; Veldhuis et al., 1997). The water temperature in shallow reef areas fluctuates widely, with daily mean values of about 25 °C in the cold season, 35 °C in the hot season. In the cold season, these shallow reef areas become dominated by zone forming algae whose biomass decreases during the hot season (Ateweberhan, 2004). 1) Department of Marine Biology and Fisheries, University of Asmara, P.O. Box 1220, Asmara, Eritrea. 2) Nationaal Herbarium Nederland, Universiteit Leiden branch, Einsteinweg 2, P.O. Box 9514, 2300 RA Leiden, The Netherlands. © 2005 Nationaal Herbarium Nederland, Leiden University branch 66 BLUMEA — Vol. 50, No. 1, 2005 The marine environment consists largely of soft substrate and shallow waters, with most areas within 50 km off the coast being less than 50 m deep. However, in some areas in the Dahlak Archipelago, the depth exceeds 200 m (Angelucci et al., 1982). The sedi- ments and rocks are largely of fossil coral reef limestone extending over the entire range of the intertidal zone. In most places in Eritrea the tidal amplitude is rather small, with an average spring tidal range of less than a metre. Horizontal platforms of fossil reef limestone formed by abrasion are common. Some of these are highly sheltered and lined at intertidal levels by convex or vertical walls. Cliffs, caves and boulders of eroded fossil limestone occur at higher intertidal levels along shores with strong wave action. In places of where a dry river (wadi) reaches the coast, these rocky limestone substrates are interrupted by terrigenous sediments or sandy covers (Lipkin, 1987, 1991). Phycological exploration Exploration of the Red Sea dates back as far as the 18th century. The first record of algae from the Red Sea was published by Strand (a student of Linnaeus) in 1756 (Papenfuss, 1968a). However, the first major algal collection was made by Forsskål (1775) during his journey to Egypt and Arabia. He described some new species from the region. Forsskål’s specimens, which are in Copenhagen, were examined by many botanists and were revised by Børgesen in 1932. The first records of algae from Eri- trea came from Ehrenberg & Hemprich who visited the Dahlak Archipelago during their six-year trip (1820–1826) to Egypt, Arabia and the western coasts of the Red Sea, including Eritrea. Hemprich died in Massawa, Eritrea. Ehrenberg did most of his work on corals but described two algal species including the famous Trichodesmium erythraeum, whose bloom is said to contribute to the colour of the Sea and hence the name (Papenfuss, 1968a; Lipkin, 1991). In the 19th century, a number of botanists, mostly Germans and Italians, visited the region and a brief history has been given by Papenfuss (1968a). Zanardini (1851) published on algae collected from the Dahlak Archipelago and Massawa and other parts of the Red Sea, describing 23 new species and a new genus (Portieria). Other new species of algae and a new genus (Sarconema) were described by him in another account on the Red Sea (Zanardini, 1858). Piccone (1884, 1886, 1889, 1893, 1900a, b, c) published seven papers dealing completely or in part with the Red Sea. Many of his new species were co-authored by A. Grunow. Especially many Sargassum taxa were described at lower taxon levels, see also Grunow (1915–1916). Licata (1882) published on the algae collected from the Assab area and De Toni & Paoletti (1888) made an account of 31 species from the region. This early stage of phycological exploration was characterized by the collection of specimens and their taxonomic and floristic treatment by Europeans, to whom little or no ecological information was available (Lipkin, 1991). The modern scientific history of the Red Sea begins with the establishment of marine research stations at Ghardaqa (Hurgada), Egypt in the 1930s and in Israel in 1968. Rayss (1959) and Rayss & Dor (1963) have added to the knowledge of the algae of the Sinai Peninsula and the Gulf of Aqaba. While marine stations were being established in the northern part of the Red Sea, the southern part remained largely unknown. Records of algae in the southern Red Sea are very scattered in literature and are based mostly on short period collections of M. Ateweberhan & W.F. Prud’homme van Reine: Seaweeds from Eritrea 67 the 20th century. Intensive collecting was carried out by the 1962 and 1965 Israel South Red Sea Expeditions, but in a limited area. Papenfuss (1968a) compiled a catalogue of previously published records of Red Sea algae, totalling 493 specific and infraspecific taxa, of which 116 (24%) were in the genus Sargassum. Collections from the Israeli expeditions were the bases of reports on Turbinaria (Taylor, 1964), Caulerpa (Taylor, 1967), Chlorodesmis (Ducker, 1967, 1969), Cystophyllum and Cystoseira (Papenfuss & Jensen, 1967), Hormophysa (Papenfuss, 1968b), Leveillea (Scagel & Chihara, 1968) and Sarconema (Papenfuss & Edelstein, 1974). Lipkin (1987) reported on the intertidal distribution of benthic marine macroalgae from Entedebir and Museri islands. An overall account of the collections made by the Israeli expeditions was only recently published (Lipkin & Silva, 2002). This account treats 127 specific and infraspecific seaweed taxa representing 73 genera. Among these algae, 13 genera and 47 species had not been recorded previously from the Red Sea. The collections came mainly from the Entedebir and Museri islands, which were the base camps of the 1962 and 1965 expeditions, respectively. Different habitats were visited within the two localities and considerable amount of time spent in field observation and collection. Most of the ecological and biogeographic suggestions about benthic algae in the southern part of the Red Sea still are biased by interpretations of patterns observed in the northern Red Sea (Walker, 1987). Seaweed distribution and biogeography of the Red Sea flora The Red Sea, which was, in the Miocene, a southern extension of the Mediterra- nean Sea, was disconnected from it geologically recently (Head, 1987). It is properly regarded as a continuation of the Indian Ocean Ridge and, effectively, a nascent ocean (Braithwaite, 1987). The origin of the fauna and flora of the Sea is essentially from the Indian Ocean, migration from and to the Mediterranean being possible only after the opening of the Suez Canal (Lipkin, 1972, 1991). The southern Red Sea, with its high salinity and warm water extending to the bottom, is oceanographically unique. The mean sea surface temperature in August is over 32 °C in the southern part of the Red Sea, and it is always c. 21.5 °C in the deeper parts (Edwards, 1987; Ateweberhan, 2004). Temperatures of 36–38 °C are very probable in the extensive shallow waters in the southern part of the Red Sea in mid summer and, in the lagoons behind the fringing reefs, readings of up to at least 45 °C have been recorded (Edwards, 1987). In Eritrea Ateweberhan (2004) reports seawater temperatures of over 36 °C in the Sargassum zone in the shallow reef flat. Average salinity in the southern Red Sea is 38 ppt, with intermittent occurrence of higher (39 ppt) or lower (36.5 ppt) values (Edwards, 1987). In the deeper parts salinity is always around 40.5 ppt (Ateweberhan, 2004). Reflecting its isolation from the Indian Ocean until about 15–20 thousand years ago, the Red Sea supports a relatively high level of endemism, including 9% for macroalgae. Proving endemism, however, requires extensive comparative collections (Head, 1987), as sound taxonomic work is a precondition for all types of biogeographical studies. Differences in physical parameters of the various parts of the Red Sea are also paralleled by dif- ferences in the biota occurring in the different regions. Species diversity increases from north to south and a marked difference in species composition can be observed along the coast extending from the northern Red Sea through the Gulf of Aden into the western Indian Ocean.
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